Jm. Li et al., FLOW BIREFRINGENCE AND COMPUTATIONAL STUDIES OF A SHEAR THINNING POLYMER-SOLUTION IN AXISYMMETRICAL STAGNATION FLOW, Journal of non-Newtonian fluid mechanics, 74(1-3), 1998, pp. 151-193
Flow of a shear thinning, moderately concentrated solution of monodisp
erse high molecular weight polystyrene has been studied in a nonhomoge
neous axisymmetric stagnation flow. Shear and extensional rheometry ha
ve been used to characterize the rheology of the solution. Multimode G
iesekus and Phan-Thien-Tanner (PTT) models, and a single mode PTT mode
l with a White-Metzner rate dependent relaxation time (PTT-WM) were fi
t to the rheological data. Transient uniaxial elongational measurement
s show significant extension hardening, which could only be predicted
by the PTT model. The Giesekus model provided the best representation
of shear flow data, but substantially underpredicted the measured exte
nsional viscosity. Flow birefringence was used to measure integrated a
xisymmetric shear and normal stress profiles as a function of position
. These measurements were compared with the results of numerical simul
ations, performed using an adaptive finite element technique, with the
three constitutive models. The computed results with the 3-mode Giese
kus model accurately portrayed experimental shear and normal stresses
in both forward and rear stagnation flow up to Weissenberg numbers (We
) of O(1). At higher We, the Giesekus model underpredicts normal stres
ses in the rear stagnation flow, where elongational gradients dominate
. Both PTT and PTT-WM models gave rise to unrealistically large extens
ional stresses in the rear stagnation flow even at moderate We which l
ed to poor agreement with experimental data. On the basis of these com
parisons, it appears that the elongational properties of the solution
are intermediate between the Giesekus and PTT, but much closer to the
Giesekus, predictions. This is in conflict with the experimentally mea
sured uniaxial viscosity, which suggests that the PTT model should be
superior in flows with significant uniaxial extension. (C) 1998 Elsevi
er Science B.V.